From Wikipedia, the free encyclopedia
The Callovian is a stage on the geologic time scale occurring 164.7 ± 4.0 Ma to 161.2 ± 4.0 Ma (million years ago). It is the last stage of the Middle Jurassic.
The stage takes its name from an old spelling of Kellaways Bridge, 3 km north-east of Chippenham in Wiltshire in England.
[edit] Geography
During the Callovian, Europe was an Archipelago of a dozen or so large islands. Between them were extensive areas of continental shelf. Consequently, there are Callovian deposits in Russia and from Belarus, through Poland and Germany, into France and eastern Spain and much of England. Around the former island coasts are frequently, land-derived sediments. These are to be found, for example, in western Scotland. (Elmi & Babin fig.55.)
[edit] Vertebrate Fauna
[edit] Crocodylomorphs
| Crocodylomorphs of the Callovian |
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The sphenosuchian Junggarsuchus was a small, ~1 meter long, Chinese predator. |
A life restoration of a Metriorhynchus species.
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An opportunistic carnivore that fed on fish, belemnites and other marine animals and possible carrion. Metriorhynchus grew to an average adult length of 3 meters (9.6 ft), although some individuals may have reached lengths rivaling those of large nile crocodiles. |
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[edit] Ornithischians
| Ornithischia of the Callovian |
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Dashanpu Formation, Sichuan, China |
A four-foot long bipedal herbivore that was built for speed. It was discovered in one of China's many Callovian deposits. |
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England |
A primitive camptosaurid iguanodont, estimated to have been 3.5 meters long |
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Kyrgyzstan |
Possibly an early pachycephalosaurid |
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Bathonian to Callovian |
Lower Shaximiao Formation, Sichuan, China |
A small ornithischian dinosaur distinguished from all other basal ornithischians by a single autapomorphy, the presence of a marked concavity that extends over the lateral surface of the postorbital. |
[edit] Plesiosaurs
| Plesiosaurs of the Callovian |
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[edit] Sauropods
[edit] Stegosauria
| Stegosaurs of the Callovian |
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Bathonian to Callovian |
Lower Shaximiao Formation, Sichuan, China |
A 4.5 meters in length quadrupedal herbivore with a small skull and a spiked tail. Bore the distinctive double row of plates, rising vertically along its arched back, of all the stegosaurians and two pairs of long spikes extending horizontally near the end of its tail |
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Lisieux, France; Northern England |
Traditionally, Lexovisaurus was depicted as having either large spines over the hips or shoulders, with a selection of flat plates and round pointed spines that ran along the back and tail. It was probably about 5 m long. |
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France; England |
Known from remains previously assigned to Lexovisaurus. |
[edit] Theropods
| theropods of the Callovian |
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A moderately large (17-23 feet long) predatory dinosaur that was closely related to Megalosaurus. |
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An 11-13 foot predator from China whose discovery was assisted by the petroleum industry. |
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A Chinese theropod that has yet to be formally described. |
[edit] Invertebrate Fauna
Members of the order ammonitda are known as Ammonitic ammonites. They are distinguished primarily by their suture lines. In ammonitic suture patterns, the lobes and saddles are much subdivided (fluted) and subdivisions are usually rounded instead of saw-toothed. Ammonoids of this type are the most important species from a biostratigraphical point of view. This suture type is characteristic of Jurassic and Cretaceous ammonoids but extends back all the way to the Permian.
| Ammonites of the Callovian |
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Life restorations of two different ammonite genera.
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[edit] Belemnites
| Belemnites of the Callovian |
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[edit] Nautiloids
| Nautiloids of the Callovian |
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An illustration of a variety of fossil nautiloids.
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[edit] Neocoleoids
| Neocoleoids of the Callovian |
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Pyritized fossil of Vampyronassa rhodanica from Voulte-sur-Rhône, France.
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A squid species discovered in France. |
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[edit] References
Serge Elmi and Claude Babin, Histoire de la Terre, 4th Edition Dunod, Paris (2002) ISBN 2 10 006631 5 (French language)